Rock Identifier
Fossiliferous limestone (Bioclastic calcarenite; predominantly calcite (CaCO₃)) — sedimentary
sedimentary

Fossiliferous limestone

Bioclastic calcarenite; predominantly calcite (CaCO₃)

AI-generated identification · may be incorrect

Typically Mohs 3, tan to cream, dull to slightly sugary/vitreous, with abundant shell fragments and possible moldic pores; calcite has rhombohedral cleavage, but grains are cemented into a rock. It appears weathered and possibly naturally rounded or worked, with dark accessory grains.

Identified More sedimentary
Explore Fossiliferous limestone in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Typically Mohs 3, tan to cream, dull to slightly sugary/vitreous, with abundant shell fragments and possible moldic pores; calcite has rhombohedral cleavage, but grains are cemented into a rock. It appears weathered and possibly naturally rounded or worked, with dark accessory grains.

Formation & geological history

Forms when marine shell debris, carbonate sand, and skeletal fragments accumulate, compact, and cement on a shallow seafloor; age cannot be determined from the image and may range from Paleozoic to Cenozoic. It may later be abraded, producing the rounded shape.

Uses & applications

Used as building stone, aggregate, cement and lime feedstock, and decorative material; attractive fossiliferous pieces are collected. This specimen has modest commercial value unless its fossils, provenance, or preparation are exceptional.

Geological facts

The white chips are likely fossil shell or skeletal fragments, commonly mollusks, echinoids, or bryozoans. Vinegar or dilute hydrochloric acid should cause visible fizzing because of calcite.

Field identification & locations

Common in former shallow tropical seas and carbonate platforms worldwide, including Florida, the Bahamas, the Mediterranean, and many European and Middle Eastern formations. Look for granular texture, visible fossils, and strong acid reaction; distinguish it from concrete by natural fossil distribution and lack of manufactured aggregate pattern.